期刊文献+

基于数字高程模型的水文模拟对比分析 被引量:12

Study of hydrological simulation on the basis of digital elevation model
下载PDF
导出
摘要 本文以GIS为平台,分析比较了不同类型的地形及网格大小的数字高程模型(DEM)所提取的汇流路径长度、坡度等地形特征值。在新安江模型参数物理意义研究的基础上,将汇流参数与地形特征值建立相关关系。利用相关关系确定参数,进行水文模拟,通过分析比较不同网格大小的DEM对水文模拟的影响。 On the platform of GIS the topographic characteristics of river basin, including the distance and slope of flood routing and slope for different kinds of landscape and different grid sizes digital elevation model (DEM) were compared. The interrationships between these characteristics and some parameters of Xinanjiang Hydrological Model were established based on the physical meaning of these parameters, and the parameters were determined consequently. The effect of DEM grid size on parameters and hydrological modeling were analyzed. It is suggested that the appropriate grid size of DEM must be determined according to the required accuracy of flood forecasting.
出处 《水利学报》 EI CSCD 北大核心 2005年第6期759-763,共5页 Journal of Hydraulic Engineering
关键词 DEM网格大小 地形特征值 流域水文模型 模型参数 DEM topographic characteristics hydrological model parameters
  • 相关文献

参考文献4

二级参考文献8

  • 1[1] Beven K J, Kirkby M J. A physical based variable contributing area model of basin hydrology[J]. Hydrol Sci Bull, 1979, 24: 43~69.
  • 2[2] Wharton G. Progress in the use of drainage network indices for rainfall-runoff modeling and runoff prediction[J]. Progress in Physical Geography, 1994, 18: 539~557.
  • 3[3] Wolock D M, McCabe Jr G J. Comparison of single and multiple flow direction algorithms for computing topographic parameters in TOPMODEL[J]. Water Resour Res, 1995, 31:945~955.
  • 4[4] Holmgren P. Multiple flow direction algorithms for runoff modelling in grid based elevation models: an empirical evaluation[J]. Hydrol Process, 1994, 8: 327~334.
  • 5[5] Soille P. Morphologie mathematique: du relief a la dimensionalite—algorithmes et methodes[D]:[Ph D thesis]. Paris: Université Catholique de Louvain & Ecole Nationale Superieure des Mines de Paris. 1992. 74~79.
  • 6[6] Hutchinson M F. A new procedure for gridding elevation and stream line data with automatic removal of spurious pits[J]. J of Hydrol, 1989, 106: 211~232.
  • 7[7] Brun C, Bernard R Vidal-Madjar D, et al. Mapping saturated areas with an helicopter-borne C-band scatterometer[J]. Water Resour Res, 1990, 26: 945~955.
  • 8李小文,王锦地.地表非同温象元发射率的定义问题[J].科学通报,1999,44(15):1612-1617. 被引量:19

共引文献111

同被引文献184

引证文献12

二级引证文献220

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部